dewpoint$550214$ - ορισμός. Τι είναι το dewpoint$550214$
Diclib.com
Λεξικό ChatGPT
Εισάγετε μια λέξη ή φράση σε οποιαδήποτε γλώσσα 👆
Γλώσσα:

Μετάφραση και ανάλυση λέξεων από την τεχνητή νοημοσύνη ChatGPT

Σε αυτήν τη σελίδα μπορείτε να λάβετε μια λεπτομερή ανάλυση μιας λέξης ή μιας φράσης, η οποία δημιουργήθηκε χρησιμοποιώντας το ChatGPT, την καλύτερη τεχνολογία τεχνητής νοημοσύνης μέχρι σήμερα:

  • πώς χρησιμοποιείται η λέξη
  • συχνότητα χρήσης
  • χρησιμοποιείται πιο συχνά στον προφορικό ή γραπτό λόγο
  • επιλογές μετάφρασης λέξεων
  • παραδείγματα χρήσης (πολλές φράσεις με μετάφραση)
  • ετυμολογία

Τι (ποιος) είναι dewpoint$550214$ - ορισμός

Dewpoint depression; Dew-point depression

Dew point depression         
The dew point depression (T-Td) is the difference between the temperature and dew point temperature at a certain height in the atmosphere.
Dew point         
TEMPERATURE AT WHICH AIR BECOMES SATURATED WITH WATER VAPOUR
Dewpoint; Frost point; Dew Point; Dew point temperature; Dewpoint temperature; Dew point factor; Due point; Dew points
The dew point is the temperature to which air must be cooled to become saturated with water vapor, assuming constant air pressure and water content. When cooled below the dew point, moisture capacity is reduced and airborne water vapor will condense to form liquid water known as dew.
dew point         
TEMPERATURE AT WHICH AIR BECOMES SATURATED WITH WATER VAPOUR
Dewpoint; Frost point; Dew Point; Dew point temperature; Dewpoint temperature; Dew point factor; Due point; Dew points
¦ noun the atmospheric temperature below which water droplets begin to condense and dew can form.

Βικιπαίδεια

Dew point depression

The dew point depression (T-Td) is the difference between the temperature and dew point temperature at a certain height in the atmosphere.

For a constant temperature, the smaller the difference, the more moisture there is, and the higher the relative humidity. In the lower troposphere, more moisture (small dew point depression) results in lower cloud bases and lifted condensation levels (LCL). LCL height is an important factor modulating severe thunderstorms. One example concerns tornadogenesis, with tornadoes most likely if the dew point depression is 20 °F (11 °C) or less, and the likelihood of large, intense tornadoes increasing as dew point depression decreases. LCL height also factors in downburst and microburst activity. Conversely, instability is increased when there is a mid-level dry layer (large dew point depression) known as a "dry punch", which is favorable for convection if the lower layer is buoyant.

As it measures moisture content in the atmosphere, the dew point depression is also an important indicator in agricultural and forest meteorology, particularly in predicting wildfires.